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首页|期刊导航|中国岩溶|两种常用染色剂管道及淤泥条件下示踪及对比 ——以丁旗地下河连通试验为例

两种常用染色剂管道及淤泥条件下示踪及对比 ——以丁旗地下河连通试验为例

易连兴 赵良杰 卢海平 王喆

中国岩溶2017,Vol.36Issue(5):721-726,6.
中国岩溶2017,Vol.36Issue(5):721-726,6.DOI:10.11932/karst2017y46

两种常用染色剂管道及淤泥条件下示踪及对比 ——以丁旗地下河连通试验为例

Comparative tracing of two common dyes in conduits with silt: A case study of the Dingqi underground river

易连兴 1赵良杰 1卢海平 1王喆1

作者信息

  • 1. 中国地质科学院岩溶地质研究所/国土资源部、广西岩溶动力学重点实验室,广西 桂林 541004
  • 折叠

摘要

Abstract

The study area is located in the upstream Dabang river,a branch of the Beipanjiang river in Dingqi town,Zhenning county,Guizhou Province.The strata of this place comprise lower Triassic limestone,dolo-mite and landform,with landforms of dissolution hills and valleys.It hosts underground rivers A19,A30 and A10,with silt deposits and buried depths less than 30 m.This study focused on the comparison of tracer experiments for two materials of Uranine and Rhodamine B,and discussion on the rationality of the recovery rates by the two methods.The results show that,(1 )The recovery rate of Uranine is 53.91%,which is higher than Rhodamine B of 40.72%;(2)Uranine's recovery intensity for maximum concentration is 2.95 times than that of Rhodamine B;(3)It is relatively easy to notice some complete wave crests in the attenua-tion section of the Rhodamine B concentration curve.It is concluded that,(1)in the underground rivers with silt deposition,Uranine and Rhodamine B have higher adsorption rates,and there may be some problems in the tracer test technology with higher recovery rates;(2)For the analysis of conduit structure or hydrogeo-logical conditions,Uranine is superior to Rhodamine B;(3)The accuracy of recovery rates depends on fluo-rimeter calibration,flow monitoring,and closely related to environmental factors,such as water-turbidity and sediments.

关键词

岩溶地下河/示踪/染色示踪剂对比/回收率

Key words

karst underground river/tracing/comparison of dyeing tracer/recovery rate

分类

天文与地球科学

引用本文复制引用

易连兴,赵良杰,卢海平,王喆..两种常用染色剂管道及淤泥条件下示踪及对比 ——以丁旗地下河连通试验为例[J].中国岩溶,2017,36(5):721-726,6.

基金项目

中国地质调查局地质调查项目"贵州打邦河流域1:5万水文地质环境地质调查"(DD20160300-02) (DD20160300-02)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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